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Soil-water characteristics of unsaturated undisturbed loess under isotropic compression condition

机译:各向同性压缩条件下不饱和不受干扰黄土的土壤 - 水特征

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Using triaxial apparatus for unsaturated soils, the isotropic compression tests at constant water content are conducted on unsaturated undisturbed loess in Xi'an under different water contents. The maximum of net confining pressure is 400 kPa. Matric suction is measured by an elevated all round air pressure and with measured pore-water pressure under zero-applied stress and applied stress. Influences of net confining pressure on matric suction characteristics of unsaturated undisturbed loess are determined and illustrated during isotropic compression at constant water content. The formula of soil-water characteristics of unsaturated undisturbed loess is obtained to determine the matric suction under zero-applied stress. Experimental results show that the influence of net confining pressure on matrix suction is related to water content. When water content is smaller than shrinkage limit, the relationship between matrix suction and net confining pressures is different from that larger than Shrinkage limit. The influence of net confining pressure is large when water content is between shrinkage limit and plastic limit, and it is slight when water content is smaller than shrinkage limit or larger than plastic limit. The relation between matric suction and degree of saturated related to net confining pressure with water content smaller than shrinkage limit is different from that related to water content. The influence of degree of saturated related to net confining pressure on matric suction is much smaller than that related to water content. Net confining pressure has relatively large influence on the relation between degree of saturated and matric suction. When net confining pressure is smaller than 400kPa, its influence on he relation between water content and matric suction is negligible, and the soil-water characteristics of undisturbed loess is illustrated by the logarithm function relation between water content and matric suction under zero-applied stress.
机译:利用三轴仪器用于不饱和土壤,在不同水质下的Xi'an中的不饱和未受干扰的黄土上进行各向同性压缩试验。净限制压力的最大值是400 KPA。在零施加应力和施加应力下,通过升高的全圆形空气压力和测量的孔隙水压测量原料抽吸。在恒定水含量的各向同性压缩期间确定和说明净狭窄压力对不饱和未受干扰黄土的测距特性的影响。得到不饱和未受干扰黄土的土壤水分特性的公式,以确定零施加应力下的测力。实验结果表明,净压力对基质吸力的影响与含水量有关。当含水量小于收缩极限时,基质抽吸和净限制压力之间的关系与大于收缩极限的关系不同。当含水量在收缩极限和塑料极限之间时,净限制压力的影响很大,当含水量小于收缩限制或大于塑料极限时,略微略微。与净限制压力的净限制与净限制的饱和压力相关的饱和度与含水量小的关系不同的关系与与水含量有关的含水含量不同。饱和程度与净狭窄压力的影响远小于与水含量有关的小得多。净限制压力对饱和度和原料吸力程度之间的关系影响相对较大。当净限制压力小于400kPa时,其对水含量和原木抽吸之间的关系的影响可忽略不计,并且不受干扰的黄土的土壤 - 水特性通过零施加应力下的水含量与原木吸力之间的对数函数关系来说明。

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